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110108

Sigma-Aldrich

cis-Pinonic acid

98%

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Synonym(s):
cis-3-Acetyl-2,2-dimethylcyclobutaneacetic acid
Linear Formula:
CH3COC4H4(CH3)2CH2CO2H
CAS Number:
Molecular Weight:
184.23
MDL number:
UNSPSC Code:
12352100
PubChem Substance ID:
NACRES:
NA.22

Assay

98%

form

solid

mp

104-107 °C (lit.)

SMILES string

CC(=O)[C@@H]1C[C@H](CC(O)=O)C1(C)C

InChI

1S/C10H16O3/c1-6(11)8-4-7(5-9(12)13)10(8,2)3/h7-8H,4-5H2,1-3H3,(H,12,13)/t7-,8+/m1/s1

InChI key

SIZDUQQDBXJXLQ-SFYZADRCSA-N

Related Categories

General description

cis-Pinonic acid undergoes oxidation to produce secondary organic aerosol (SOA).

Pictograms

Exclamation mark

Signal Word

Warning

Hazard Statements

Hazard Classifications

Eye Irrit. 2 - Skin Irrit. 2 - STOT SE 3

Target Organs

Respiratory system

WGK

WGK 3

Flash Point(F)

Not applicable

Flash Point(C)

Not applicable

Personal Protective Equipment

dust mask type N95 (US), Eyeshields, Gloves

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Yuanlong Huang et al.
The journal of physical chemistry. A, 122(31), 6445-6456 (2018-07-17)
Gas and aqueous phases are essential media for atmospheric chemistry and aerosol formation. Numerous studies have focused on aqueous-phase reactions as well as coupled gas/aqueous-phase mass transport and reaction. Few studies have directly addressed processes occurring at the air-water interface
Andrea Arangio et al.
Applied spectroscopy, 73(6), 638-652 (2019-04-17)
The application of electrospray (ES) for quantitative transfer of analytes from solution to an internal reflection element for analysis by attenuated total reflection Fourier transform infrared (ATR FT-IR) spectroscopy has been developed in this work. The ES ATR FT-IR method
Fragmentation vs. functionalization: chemical aging and organic aerosol formation.
Chacon-Madrid HJ and Donahue NM.
Atmospheric Chemistry and Physics, 11(20), 10553-10563 (2011)
Emma Q Walhout et al.
Environmental science & technology, 53(13), 7604-7612 (2019-06-12)
Characterizing the chemical composition of organic aerosols can elucidate aging mechanisms as well as the chemical and physical properties of the aerosol. However, the high chemical complexity and often low atmospheric abundance present a difficult analytical challenge. Milligrams or more
Markus Müller et al.
Analytical chemistry, 89(20), 10889-10897 (2017-09-16)
We report on a new method for analyzing atmospheric submicrometer particulate organic matter which combines direct particle sampling and volatilization with online chemical ionization mass spectrometric analysis. Technically, the method relies on the combined use of a CHARON ("Chemical Analysis

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